High School Living Earth Evidence for Evolution Lessons Name: School: Teacher
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Distinguishing Quaternary Glyptodontine Cingulates in South America: How Informative Are Juvenile Specimens?
Distinguishing Quaternary glyptodontine cingulates in South America: How informative are juvenile specimens? CARLOS A. LUNA, IGNACIO A. CERDA, ALFREDO E. ZURITA, ROMINA GONZALEZ, M. CECILIA PRIETO, DIMILA MOTHÉ, and LEONARDO S. AVILLA Luna, C.A., Cerda, I.A., Zurita, A.E., Gonzalez, R., Prieto, M.C., Mothé, D., and Avilla, L.S. 2018. Distinguishing Quaternary glyptodontine cingulates in South America: How informative are juvenile specimens? Acta Palaeontologica Polonica 63 (1): 159–170. The subfamily Glyptodontinae (Xenarthra, Cingulata) comprises one of the most frequently recorded glyptodontids in South America. Recently, the North American genus Glyptotherium was recorded in South America, in addition to the genus Glyptodon. It has been shown that both genera shared the same geographic distribution in central-north and eastern areas of South America (Venezuela and Brazil, respectively). Although some characters allow differentiation between adult specimens of both genera, the morphological distinction between these two genera is rather difficult in juvenile specimens. In this contribution, a detailed morphological, morphometric and histological survey of a juvenile specimen of Glyptodontinae recovered from the Late Pleistocene of northern Brazil is performed. The relative lower osteoderms thickness, the particular morphology of the annular and radial sulci and the distal osseous projections of the caudal osteoderms suggest that the specimen belongs to the genus Glyptotherium. In addition, the validity of some statistical tools to distinguish between different ontogenetic stages and in some cases between genera is verified. The osteoderm microstructure of this juvenile individual is characterized by being composed of a cancellous internal core surrounded by a compact bone cortex. Primary bone tissue mostly consists of highly vascularized, woven-fibered bone tissue. -
Mammalia, Cingulata, Glyptodontia)
Journal of South American Earth Sciences 66 (2016) 32e40 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames A reassessment of the taxonomic status of Paraglyptodon Castellanos, 1932 (Mammalia, Cingulata, Glyptodontia) * Laura E. Cruz a, , Juan C. Fernicola a, b, Matias Taglioretti c, Nestor Toledo d a CONICET, Consejo Nacional de Investigaciones Científicas y Tecnicas-Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”,Av.Angel Gallardo 470, Capital Federal, C1405DJR, Argentina b Departamento de Ciencias Basicas, Universidad Nacional de Lujan, Ruta 5 y Avenida Constitucion, 6700, Lujan, Buenos Aires, Argentina c CONICET-Instituto de Geología de Costas y del Cuaternario, Facultad de Ciencias Exactas y Naturales, Universidad Nacional de Mar del Plata, Dean Funes 3350, B7602AYL, Mar del Plata, Buenos Aires, Argentina d CONICET-Division Paleontología Vertebrados, Unidades de Investigacion Anexo Museo FCNyM-UNLP, Avenida 60 y 122, B1900FWA, La Plata, Argentina article info abstract Article history: Castellanos described and published about new genera of glyptodonts, according to a phylogenetic Received 21 September 2015 scheme mainly based on the evolution of the external surface of the dorsal carapace. Among these new Received in revised form genera, Castellanos proposed Paraglyptodon as the predecessor of Glyptodon, and included within Par- 4 November 2015 aglyptodon all known species of Glyptodontinae recovered from “horizontes pre-Ensenadenses”, and Accepted 20 November 2015 within Glyptodon all known species from “Horizontes pampeanos”, restricting the latter to the Quaternary. Available online 25 November 2015 All the species that belong to Paraglyptodon, that is Paraglyptodon chapalmalensis, Paraglyptodon uquiensis, Paraglyptodon dubius, and Paraglyptodon paranensis were established based on one, two or few Keywords: Osteoderm osteoderms, mostly from the dorsal carapace. -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
Transitional Fossils by Greg
Transitional Fossils By Greg Neyman © Answers In Creation Answers In Creation Website www.answersincreation.org/transitional_fossils.htm Transitional fossils, or the supposed lack thereof, has been used for many years by anti-evolutionists to argue against evolution. Here, I will explain what a transitional fossil is, and why it is not valid as an argument against evolution. A transitional fossil shows the evolutionary development from one species to another. For example, if organism 1 existed 70 million years ago, and organism 2 shows up in the fossil record 5 million years later, then theoretically there should be intermediate species in this 5 million year gap, which shows gradual progression from one species to another. The lack of these "transitional" fossils is proof to young earth creationists that evolution is false. Evolutionists have shown that indeed there are transitional fossils, and there are plenty of examples of them. For instance, see http://www.talkorigins.org/faqs/faq- transitional.html . Here is the key point...even if young earth creationists accept these examples of transitional fossils, they will still claim that there are no transitional fossils! These fossils will be called either unique species, or they will come up with some reason (disease, birth defect, etc) that accounts for the apparent transition feature. Naturally, they will say, "Where are the transitional fossils between these transitional fossils?" If we had a clear fossil record, showing progression every 10,000 years for millions of years, they will not believe it, and will want the "transitional" fossils for the missing 10,000 year period. No amount of evidence will convict them that their belief is wrong. -
New Transitional Fossil from Late Jurassic of Chile Sheds Light on the Origin of Modern Crocodiles Fernando E
www.nature.com/scientificreports OPEN New transitional fossil from late Jurassic of Chile sheds light on the origin of modern crocodiles Fernando E. Novas1,2, Federico L. Agnolin1,2,3*, Gabriel L. Lio1, Sebastián Rozadilla1,2, Manuel Suárez4, Rita de la Cruz5, Ismar de Souza Carvalho6,8, David Rubilar‑Rogers7 & Marcelo P. Isasi1,2 We describe the basal mesoeucrocodylian Burkesuchus mallingrandensis nov. gen. et sp., from the Upper Jurassic (Tithonian) Toqui Formation of southern Chile. The new taxon constitutes one of the few records of non‑pelagic Jurassic crocodyliforms for the entire South American continent. Burkesuchus was found on the same levels that yielded titanosauriform and diplodocoid sauropods and the herbivore theropod Chilesaurus diegosuarezi, thus expanding the taxonomic composition of currently poorly known Jurassic reptilian faunas from Patagonia. Burkesuchus was a small‑sized crocodyliform (estimated length 70 cm), with a cranium that is dorsoventrally depressed and transversely wide posteriorly and distinguished by a posteroventrally fexed wing‑like squamosal. A well‑defned longitudinal groove runs along the lateral edge of the postorbital and squamosal, indicative of a anteroposteriorly extensive upper earlid. Phylogenetic analysis supports Burkesuchus as a basal member of Mesoeucrocodylia. This new discovery expands the meagre record of non‑pelagic representatives of this clade for the Jurassic Period, and together with Batrachomimus, from Upper Jurassic beds of Brazil, supports the idea that South America represented a cradle for the evolution of derived crocodyliforms during the Late Jurassic. In contrast to the Cretaceous Period and Cenozoic Era, crocodyliforms from the Jurassic Period are predomi- nantly known from marine forms (e.g., thalattosuchians)1. -
Late Cenozoic Large Mammal and Tortoise Extinction in South America
Cione et al: Late Cenozoic extinction Rev.in South Mus. America Argentino Cienc. Nat., n.s.1 5(1): 000, 2003 Buenos Aires. ISSN 1514-5158 The Broken Zig-Zag: Late Cenozoic large mammal and tortoise extinction in South America Alberto L. CIONE1, Eduardo P. TONNI1, 2 & Leopoldo SOIBELZON1 1Departamento Científico Paleontología de Vertebrados, 'acultad de Ciencias Naturales y Museo, Paseo del Bosque, 1900 La Plata, Argentina. 2Laboratorio de Tritio y Radiocarbono, LATYR. 'acultad de Ciencias Naturales y Museo, Paseo del Bosque, 1900 La Plata, Argentina. E-mail: [email protected], [email protected], [email protected]. Corresponding author: Alberto L. CIONE Abstract: During the latest Pleistocene-earliest Holocene, South American terrestrial vertebrate faunas suffered one of the largest (and probably the youngest) extinction in the world for this lapse. Megamammals, most of the large mammals and a giant terrestrial tortoise became extinct in the continent, and several complete ecological guilds and their predators disappeared. This mammal extinction had been attributed mainly to overkill, climatic change or a combination of both. We agree with the idea that human overhunting was the main cause of the extinction in South America. However, according to our interpretation, the slaughtering of mammals was accom- plished in a particular climatic, ecological and biogeographical frame. During most of the middle and late Pleis- tocene, dry and cold climate and open areas predominated in South America. Nearly all of those megamammals and large mammals that became extinct were adapted to this kind of environments. The periodic, though rela- tively short, interglacial increases in temperature and humidity may have provoked the dramatic shrinking of open areas and extreme reduction of the biomass (albeit not in diversity) of mammals adapted to open habitats. -
Measuring the Impact of Extinct Megafauna on Carbon Fluxes in Ponderosa Pine Forests
Impact of Extinct Megafauna on Carbon Fluxes | EGM-5 APPLICATION NOTE Measuring the Impact of Extinct Megafauna on Carbon Fluxes in Ponderosa Pine Forests It is increasingly recognized that animals are not simply passive recipients of a world organized by powerful non-living forces such as climate, soil and fire. Instead they are key actors, exerting their own biological control on the composition and function of ecosystems across the world. It is likely that the importance of animals as agents of global change has been overlooked until recently because today we live in a world devoid of most of its megafauna (Sandom et al., 2014). Since the late Pleistocene, megafauna populations have been in a state of decline worldwide and today we have unequivocally entered the sixth mass extinction (Malhi et al., 2016). Both human and climatic reasons have been forwarded to explain the dramatic declines in megafauna populations, and whilst this has been the subject of intense debate (e.g. Johnson, 2002; Barnosky et al., 2004), there has been little conversation about the legacies of these lost ecosystem engineers across the world. Figure 1: Normalized Difference Vegetation Index (NDVI) drone imagery for plots 2 (left) and 3 (right) (greyscale) overlaid on a Google maps image showing the forest thinning. Plot two is representative of a past landscape containing megaherbivores and without fire suppression. In the present study, we aim to understand how past megafauna influenced carbon cycling in Ponderosa pine forests. Megaherbivores – by their sheer size – consume a vast amount of vegetation and cause widespread structural damage to woody plants. -
The Brazilian Megamastofauna of the Pleistocene/Holocene Transition and Its Relationship with the Early Human Settlement of the Continent
Earth-Science Reviews 118 (2013) 1–10 Contents lists available at SciVerse ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev The Brazilian megamastofauna of the Pleistocene/Holocene transition and its relationship with the early human settlement of the continent Alex Hubbe a,b,⁎, Mark Hubbe c,d, Walter A. Neves a a Laboratório de Estudos Evolutivos Humanos, Departamento de Genética e Biologia Evolutiva, Instituto de Biociências, Universidade de São Paulo, Rua do Matão 277, São Paulo, SP. 05508-090, Brazil b Instituto do Carste, Rua Barcelona 240/302, Belo Horizonte, MG. 30360-260, Brazil c Department of Anthropology, The Ohio State University, 174W 18th Avenue, Columbus, OH. 43210, United States d Instituto de Investigaciones Arqueológicas y Museo, Universidad Católica del Norte, Calle Gustavo LePaige 380, San Pedro de Atacama, 141-0000, Chile article info abstract Article history: One of the most intriguing questions regarding the Brazilian Late Quaternary extinct megafauna and Homo Received 4 October 2012 sapiens is to what extent they coexisted and how humans could have contributed to the former's extinction. Accepted 18 January 2013 The aim of this article is to review the chronological and archaeological evidences of their coexistence in Available online 25 January 2013 Brazil and to evaluate the degree of direct interaction between them. Critical assessment of the Brazilian megafauna chronological data shows that several of the late Pleistoscene/early Holocene dates available so Keywords: far cannot be considered reliable, but the few that do suggest that at least two species (Catonyx cuvieri, Quaternary Mammals ground sloth; Smilodon populator, saber-toothed cat) survived until the beginning of the Holocene in Southeast Extinction Brazil. -
Evidence for Evolution
CHAPTER 3 Evidence for Evolution VOLUTIONARY BIOLOGY HAS PROFOUNDLY altered our view of nature and of ourselves. At the beginning of this book, we showed the practical application of Eevolutionary biology to agriculture, biotechnology, and medicine. More broadly, evolutionary theory underpins all our knowledge of biology, explains how organisms came to be (both describing their history and identi- fying the processes that acted), and explains why they are as they are (why organisms reproduce sexually, why they age, and so on). How- ever, arguably its most important influence has been on how we view ourselves and our place in the world. The radical scope of evolution- ary biology has for many been hard to accept, and this has led to much misunderstanding and many objections. In this chapter, we summarize the evidence for evolution, clarify some common misun- derstandings, and discuss the wider implications of evolution by natural selection. Biological evolution was widely accepted soon after the publication of On the Origin of Species in 1859 (Chapter 1.x). Charles Darwin set out “one long argument” for the “descent with modification” of all liv- ing organisms, from one or a few common ancestors. He marshaled evidence from classification of organisms, from the fossil record, from geographic distribution of organisms, and by analogy with artificial se- lection. As we saw in Chapter 1, the detailed processes that cause evo- lution remained obscure until after the laws of heredity were established in the early 20th century. By the time of the Evolutionary Synthesis,in the mid-20th century, these processes were well understood and, cru- cially, it was established that adaptation is due to natural selection (Chapter 1.x). -
Memoir on the Megatherium, Or Giant Ground-Sloth of America
':-., .i>m;'-. •.,!:::;:•. " ••'"•' -v- Mi .;..;...: EffiWnfis K '•'•;. "".ll . Bill tdflKHfci .V ..:'•',; mmM (<W ' '&5?'}f!'LjijnF» ' * f . c«*Rl«(l — ® MEMOIR ON THE MEGATHERIUM, OR GIANT GROUND-SLOTH OF AMERICA (Megatherium umericanum, Cuvier). by RICHARD OWEN, F.R.S., D.C.L., SUPERINTENDENT OF THE NATURAL HISTORY DEPARTMENTS IN THE BRITISH MUSEUM ; . FULLERIAN PBOFB8SOB OF PHYSIOLOGY IN THE ROTAL INSTITUTION OF GREAT BRITAIN ; FOREIGN ASSOCIATE OF THE INSTITUTE OF FRANCE, ETC. WILLIAMS AND NORGATE, 14. HENEIETTA STEEET, COVENT GAEDEN, LONDON; AND 20, SOUTH FEEDEEICK STEEET, EDINBUEGH. 1861. TO THE ROYAL SOCIETY OF LONDON, This Work, which owes its origin to the Society's favourable reception of the Authors commwiications on the Megatherium, and allied fossils, in the years 1851 and 1855, and the drawings for its illustration chiefly to the liberal application thereto of part of the 'Government Grant,' is, by permission of the President and Council, most gratefully and respectfully dedicated, by THE AUTHOR. CONTENTS. Pafte 3 § 1. Historical Introduction 12 § 2. Of the Spinal Column § 3. Comparison of the Spinal Column 25 § 4. Of the Skull 28 § 5. Of the Teeth 36 § 6. Comparison of the Skull and Dentition 41 § 7. Of the Bones of the Anterior Extremity 45 § 8. Of the Bones of the Posterior Extremity 62 § 9. Comparison of the Bones of the Hind-foot 74 §10. Physiological Summary 77 §11. Geological Summary ^2 DESCRIPTION OF THE SKELETON OF THE MEGATHERIUM. ^ 1. Historical Introduction. JjEFORE commencing the description of the skeleton of the Megatherium, now in London, Plate I., which is the most complete that has yet reached Europe, a brief statement may be premised of the chief steps which have led to the restoration of the species (Megatherium Americanum, Cuvier and Blumenbach) to which it belongs. -
A Brief History of Whale Evolution: As Supported by The
A Brief History of Whale Evolution As Supported By the Fossil Record BIOB 272 – Genetics and Evolution Presented by Mindy Flanders Presented for Rick Henry December 8, 2017 Cetaceans—whales, dolphins, and porpoises—are so different from other animals that, until recently, scientists were unable to identify their closest relatives. As any elementary student knows, a whale is not a fish. That means that despite the similarities in where they live and how they look, whales are not at all like salmon or even sharks. Carolus Linnaeus, known for classifying plants and animals, noted in the 1750s that “whales breathe air through lungs not gills; are warm blooded; and have many other anatomical differences that distinguish them from fish” (Prothero, 2015). Other characteristics cetaceans share with all other mammals are: they have hair (at some point in their life), they give birth to live young, and they nurse their young with milk. This implies that whales evolved from other mammals and, because ancestral mammals were land animals, that whales had land ancestors (Thewissen & Bajpai, 2001). But before they had land ancestors they had water ancestors. The ancestors of fish lived in water, too. Up until 375 million years ago (mya), everything other than plants and insects lived in water, but it was around that time that fish and land animals began to diverge. A series of fossils represent the fish-to-tetrapod transition that occurred during the Late Devonian Period 359-383 mya (Herron & Freeman, 2014). In search of a new food source, or to escape predators more than twice their size (Prothero, 2015), the first tetrapods pushed themselves out of the swamps and began to live on land (Switek, 2010). -
Explore Your Inner Animals Worksheet
TEACHER MATERIALS EXPLORE YOUR INNER ANIMALS WORKSHEET OVERVIEW This worksheet accompanies the Click & Learn “Explore Your Inner Animals” (http://www.hhmi.org/biointeractive/explore- your-inner-animals). As they work through the Click & Learn, students explore multiple lines of evidence for common descent found among the bodies and cells of both extinct and extant organisms. This content was also featured in the film Your Inner Fish and in the Great Transitions: The Origin of Tetrapods short film. Visit http://www.hhmi.org/biointeractive/your-inner-fish for more information. The student worksheet is designed to help ensure students successfully navigate the interactive and can be completed in class or assigned as homework. Students may complete all of the different sections or only some of them. KEY CONCEPTS AND LESSON OBJECTIVES • Species descend from other species. Even distantly related species, like humans and sponges, can trace their shared ancestry back to a common ancestor. • Evidence for common descent includes the fossil record and anatomical, genetic, and developmental homologies among organisms. • The fossil record provides a history of life on Earth. It includes fossils with features that are intermediate, or transitional, between those of major groups of animals. • When a series of transitional fossils are viewed together, they reveal the gradual sequence of change connecting one major group to another. • An organism’s DNA codes for proteins that result in an organism’s visible traits. • Scientists infer function and behavior from anatomical structures. • Natural selection is the process by which heritable traits that confer a survival and/or reproductive advantage to individuals that possess them increase in frequency within a population over generations.